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dc.contributor.authorGiménez, R.
dc.contributor.authorVilas, Lorenzo
dc.description.abstractDuring Late Cenomanian, an Atlantic transgression occurs as a result of the Iberian Plate tilting. Its southern limit is recognized in the Murcia-Albacete-Valencia area, with continental sediments, which are dividing the Iberian and Betic basins during that agees_ES
dc.publisherSociedad Geológica de Españaes_ES
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 España*
dc.subject.otherTransgression boundaryes_ES
dc.subject.otherLate Cenomanianes_ES
dc.subject.otherIberian and Betic Rangeses_ES
dc.titleEl límite meridional de la transgresión cenomaniense superior en la Cordillera Ibérica (Murcia, Albacete y Valencia)es_ES

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Atribución-NoComercial-SinDerivadas 3.0 España
Except where otherwise noted, this item's license is described as Atribución-NoComercial-SinDerivadas 3.0 España

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